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Tegulavis corbalani nov. gen., nov. sp.; Papulavis annae nov. gen., nov. sp. (2 Viewers)

Fred Ruhe

Well-known member
Netherlands
Cécile Mourer-Chauviré, Estelle Bourdon, Sylvain Duffaud, Guy Le Roux, Yves Laurent, 2024

New avian remains from the early Eocene of La Borie, southern France


Geobios, Volume 83, April 2024, Pages 61-84

Abstract: https://www.sciencedirect.com/science/article/abs/pii/S0016699523000050

The giant flightless bird Gastornis laurenti Mourer-Chauviré and Bourdon, 2020, has been described from a mandible, maxilla and quadrate discovered in the early Eocene locality of La Borie (middle Ypresian, reference level MP 8–9). This locality has yielded abundant fossil vertebrates. We describe here new postcranial remains of G. laurenti, a coracoideum assigned to Tegulavis corbalani nov. gen., nov. sp. (cf. Galliformes), a tarsometatarsus attributed to Papulavis annae nov. gen., nov. sp. (cf. Aramidae), and the tibiotarsus of a small gruiform related to either Walbeckornis or Messelornithidae. The study of the postcranial material confirms that the species G. laurenti differs from other species of Gastornis in many features. The avifauna from La Borie is not very diversified but matches well with the paleoenvironment, which consists of an alluvial flood plain with sparse vegetation, in a tropical climate.

Enjoy,

Fred
 
Systematic palaeontolog

Class Aves Linnaeus, 1758
Cf. Order Galliformes Temminck, 1820
Family Incertae Sedis
Genus Tegulavis nov.
LSID of new genus: 3EDA11B9-F0FE-4CB7-808AFDB45019D3D0

Derivation of the name: From tegula, Latin name of tiles that
are produced with the clay excavated in the La Borie quarry, and
avis, bird.

Type and only species: Tegulavis corbalani nov.gen., nov. sp.

Stratigraphic and geographic occurrence: Ypresian (early Eocene), southern France.

Diagnosis: As for the type species Tegulavis corbalani, by monotypy.

Type locality:
La Borie, Saint-Papoul, Department of Aude,
southern France.

Type horizon: Middle Ypresian, early Eocene, reference-level
MP 8–9, age ca. 53–52 Ma (Danilo et al., 2013)

Measurements (in mm): Medial length (from omal end to
angulus medialis)
, 41.7; omal width (from medial side of cotyla
scapularis to lateral side of fac. art. hum.), 8.5; omal width (measured obliquely from fac. art. clavicularis to lateral border of fac. art. hum.), 11.2; omal depth (at the level of cotyla scap.), 6.8;
mid-shaft width, 4.2; mid-shaft depth, 3.5; sternal width, as eserved, 17.1; sternal depth, as preserved, 3.5.

Differential diagnosis:
The coracoideum of Tegulavis exhibits
the following characteristics: very deep, subcircular cotyla scapularis; facies articularis humeralis strongly projecting laterally;
absence of processus procoracoideus and foramen nervi supracoracoidei. These features also occur in the stem group galliforms Quercymegapodiidae, Gallinuloididae and Paraortygidae. However, Tegulavis differs from these taxa mainly in the morphology of the sternal end: both sides of sternal end symmetrical, facies articularis sternalis almost rectilinear, absence of pneumatic foramen and lineae intermusculares on the dorsal surface, presence of wide and rounded keel on the ventral surface. In contrast, in the other families, the sternal end is wider laterally, the facies articularis sternalis is curved, and the ventral surface is flat.

Remarks: Comparison with the Quercymegapodiidae. The family Quercymegapodiidae was described from the middle (MP 16) and late (MP 17 to 19) Eocene of the Phosphorites du Quercy, France
(Mourer-Chauviré, 2006), based on the genus Quercymegapodius.
An omal part of coracoideum is known for the species ercymegapodius depereti (Gaillard, 1908) and Quercymegapodius brodkorbi Mourer-Chauviré, 1992 (fig. 1d, e, t, u). Tegulavis nov. gen. resembles Quercymegapodius in the following characteristics: deep subcircular cotyla scap. and laterally projecting fac. art. hum.;
absence of processus procoracoideus and foramen n. pracoracoidei. However, in Tegulavis nov. gen., the fac. art. hum. is more laterally expanded, the processus acrocoracoideus is less curved in sternal direction, and the cotyla scap. is more developed on the medial side. In Q. depereti the medial and lateral sides of the shaft are almost parallel and diverge only slightly in sternal direction, whereas in Tegulavis nov. gen. the margins of the shaft are more divergent sternally. In Tegulavis nov. gen. there is a deep
groove on the lateral surface, between the fac. art. hum. and the
shaft, while this groove is shallower in Quercymegapodius. The family Quercymegapodiidae also includes the genus Ameripodius, from the late Oligocene or early Miocene of Brazil, and early Miocene of France, and the genus Taubacrex, from the late Oligocene or early Miocene of Brazil (Alvarenga, 1988, 1995; Mourer-Chauviré, 2000). Tegulavis nov. gen. differs from Ameripodius mainly in the sternal part of the coracoideum. In Ameripodius, the fac. art. sternalis is laterally elongate and oblique relative to the long axis of the shaft, while in Tegulavis nov. gen. the sternal part is almost bilaterally symmetrical and the fac. art. ernalis is roughly perpendicular to the long axis of the shaft. In Ameripodius silvasantosi Alvarenga, 1995, the impressio m. sternocoracoidei shows a strong oblique linea intermuscularis and a large pneumatic foramen. In Ameripodius alexis Mourer-Chauviré, 2000, there are several oblique parallel lineae intermusculares, and the pneumatic foramen is more rounded. In Tegulavis nov. gen., the fac. art. hum is extended by the impressio lig. acrocoracohumeralis and processus acrocoracoideus, the whole structure forming an arch in dorsal view. In contrast, in the Quercymegapodiidae, a notch occurs between the fac. art. hum. and the processus acrocoracoideus, at the level of the impressio lig. acrocoracohumeralis. In the Quercymegapodiidae, the processus acrocoracoideus exhibits a prominent tubercle on the ventral surface, but this part is incompletely preserved in Tegulavis nov. gen. Several omal parts of coracoideum have been reported from the early Eocene of Mongolia (Bumban Mb. of the Tsagaan Khushuu locality). The first specimen has been referred to cf. Quercymegapodiidae gen. and sp. indet (Hood et al. 2019). Two other coracoidea have been attributed to the new genera
and species Bumbanortyx transitoria Zelenkov, 2021, and Bumbanipodius magnus Zelenkov, 2021, respectively (Zelenkov, 2021a). These genera are considered as Galliformes incertae familiae but show similarities with the families Gallinuloidae and Quercymegapodiidae. Tegulavis nov. gen. differs from these smallsized Mongolian forms in the following features: fac. art. hum.
more prominent laterally, absence of processus procoracoideus,
impressio lig. acrocoracohumeralis more developed, processus
acrocoracoideus less curved, lateral and medial sides of the shaft
more divergent. The species Ludiortyx hoffmanni (Gervais, 1852),
from the late Eocene of the Paris Basin, has been tentatively
assigned to the Quercymegapodiidae on several occasions (Mayr,
2000, 2005, 2009; Tomek et al., 2014). Unfortunately, it is not possible to compare Tegulavis nov. gen. with Ludiortyx, since it is not possible to see the morphological details of the coracoidea on the material attributed to the latter genus.
Comparison with the Palintropiformes. The genus Palintropus,
including the species P Palintropus retusus (Marsh, 1892), has been
described based on an omal part of left coracoideum from the
upper Cretaceous (Late Maastrichtian) of the Lance Fm., Wyoming,
USA. Two other omal parts of coracoideum are known from the
Campanian of Alberta, Canada, and are assigned to Palintropus sp.
A and Palintropus sp. B (Longrich, 2009). Hope (2002) put this
genus in ?Galliformes?Quercymegapodiidae, then Longrich et al.
(2011) placed it in its own order Palintropiformes. A cladistics
analysis showed that Palintropus is the sister taxon of the archaic
ornithurine Apsaravis, from the late Campanian to early Maastrichtian of Mongolia (Clarke and Norell, 2002). The genus Palintropus is characterized by a fac. art. hum. that strongly projects
laterally, a circular cotyla scap., the absence of processus ocoracoideus, and the presence of a wide foramen n. pracoracoidei in central position on the shaft and distant from the cotyla scap. Hope (2002) indicates that this foramen distinguishes Palintropus from the Quercymegapodiidae. The other orphological characteristics of Palintropus are the presence of a depression on the dorsal surface of the coracoideum, and a longitudinal groove on the medial surface of the coracoideal shaft. The foramen n. supracoracoidei passes through the dorsal depression into the medial depression (Longrich et al., 2011: suppl. inf. p. 8). The processus acrocoracoideus is relatively short and slightly hooked medially around the sulcus m. supracoracoidei. The coracoideum of Apsaravis resembles that of Palintropus in the concave cotyla scap., the flange-like, ventrally curved fac. art. hum., and the loss of the processus procoracoideus. It also shows a dorsal fossa with the opening of the foramen n. supracoracoidei and a very elongate groove on the medial face with the opposite opening of this foramen. Tegulavis nov. gen. resembles Palintropu nd Apsaravis in the concave subcircular cotyla scap., the fac. art. hum. that strongly projects laterally, and the absence of processus procoracoideus. Tegulavis nov. gen. differs from these taxa in the absence of dorsal fossa, foramen n. supracoracoidei, and longitudinal groove on the medial face. In addition, the processus acrocoracoideus of Tegulavis nov. gen. is more elongate and more strongly hooked in medial direction than in Palintropus and Apsaravis. The sternal part and the ventral surface are visible in Apsaravis ukhaana Clarke and Norell, 2002 (figs. 12-15). The ventral surface is flat, the fac. art. sternalis is obliquely oriented relative to the long axis of the shaft, and the processus lateralis is well developed (Clarke and Norell, 2002: fig. 13), whereas in Tegulavis nov. gen. the ventral surface shows a keel, the fac. art. sternalis is almost perpendicular to the long axis of the shaft, and the processus lateralis seems poorly developed.
Comparison with the Gallinuloididae and Paraortygidae. The
Gallinuloididae are present in the early Eocene of North America
and Europe, with the genera Gallinuloides and Paraortygoides
(Mayr, 2000, 2006; Mayr and Weidig, 2004; Weidig, 2010). The
Paraortygidae are present in the late Eocene to late Oligocene of
the Phosphorites du Quercy (Mourer-Chauviré, 1992, 2006), early
Oligocene of Germany (Fischer, 1990, 2003) and Belgium (Mayr
and Smith, 2013), with the genera Paraortyx and Pirortyx; the middle Eocene of Namibia (Mourer-Chauviré et al., 2015, 2017), with the genus Scopelortyx; the middle Eocene of Uzbekistan
(Zelenkov and Panteleyev, 2019), with the genus Xorazmortyx;
the middle Eocene of USA (Stidham et al., 2020) with a fragment
of coracoideum, gen. and sp. indet. The coracoidea of the Gallinuloididae and Paraortygidae are very close morphologically and Tegulavis nov. gen. differs from these taxa in the same characters. In the Gallinuloididae and Paraortygidae, the coracoideum shows a cup-like, concave, circular or slightly ellipsoidal cotyla scap. and a very short processus procoracoideus (Mayr, 2000, 2006). Tegulavis nov. gen. differs from these taxa in the following features: the cotyla scap. is not circular, the processus procoracoideus is absent, and the processus acrocoracoideus is shorter in omal and medial direction. In the sternal part, the coracoideum of the Gallinuloididae and Paraortygidae shows oblique lineae intermusculares, the processus lateralis is more elongate than the angulus medialis, and the fac. art. sternalis is strongly curved. In Tegulavis nov. gen., there are no lineae intermusculares, the sternal part is almost bilaterally symmetrical, and the fac. art. sternalis is rectilinear. In Gallinuloididae and Paraortygidae, there is no deep groove between the fac. art. hum. and the lateral side of the shaft, and the ventral surface is flat (Mayr and Weidig, 2004: fig. 4), whereas in Tegulavis nov. gen. there is a deep groove and the ventral surface is convex. Comparison with the genera Argillipes, Nanortyx, and Sobniogall . A coracoideum from the early Eocene locality of Egem, in Belgium, has been described as aff. Argillipes aurorum Harrison and Walker, 1977, family incertae sedis. This locality is coeval with La Borie (Mayr and Smith, 2019a). In this coracoideum, the tip of the processus procoracoideus is broken. The fac. art. scap. is concave and circular, but the fac. art. hum. is much less laterally prominent than in Tegulavis nov. gen. This bone differs from Tegulavis nov. gen. in three additional features: the shaft is narrow and elongate; there are muscle scars in the impressio m. sternocoracoidei; a marked bulge is present in the sulcus m. supracoracoidei, just omal of the fac. art. scap. Furthermore, this coracoideum is almost twice smaller than that of Tegulavis nov. gen. The genus Nanortyx, with the species Nanortyx inexpectatus Weigel, 1963, has been described from the late Eocene of Canada. It was assigned to the family Odontophoridae, but this attribution has not been confirmed (Weigel, 1963; Mayr, 2009, 2017a). The coracoideum is not well preserved in this species. The fac. art. scap. is circular and concave, as in Tegulavis nov. gen. In contrast to the latter species, the coracoideum of Nanortyx shows a prominent processus procoracoideus that projects dorsally, and a fac. art. hum. that weakly protrudes laterally.Sobniogallus albinojamrozi Tomek et al., 2014 is a Galliforme, Family incertae sedis, described from the early Oligocene of Poland. Tegulavis nov. gen. resembles this genus in the laterally protruding fac. art. hum., which is separated 1
from the shaft by a deep groove on the lateral surface. However,
in Sobniogallus, the processus acrocoracoideus is obliquely
directed, strongly projecting omally, and not hooked in sternal
direction (Tomek et al., 2014: fig. 3-2 Comparison with the genera Argillipes, Nanortyx, and Sobniogallus. A coracoideum from the early Eocene locality of Egem, in Belgium, has been described as aff. Argillipes aurorum Harrison and Walker, 1977, family incertae sedis. This locality is coeval with La Borie (Mayr and Smith, 2019a). In this coracoideum, the tip of the processus procoracoideus is broken. The fac. art. scap. is concave and circular, but the fac. art. hum. is much less laterally prominent than in Tegulavis nov. gen. This bone differs from Tegulavis nov. gen. in three additional features: the shaft is narrow and elongate; there are muscle scars in the impressio m. sternocoracoidei; a marked bulge is present in the sulcus m. supracoracoidei, just omal of the fac. art. scap. Furthermore, this coracoideum is almost twice smaller than that of Tegulavis nov. gen. The genus Nanortyx, with the species Nanortyx inexpectatus Weigel, 1963, has been described from the late Eocene of Canada. It was assigned to the family Odontophoridae, but this attribution has not been confirmed (Weigel, 1963; Mayr, 2009, 2017a). The coracoideum is not well preserved in this species. The fac. art. scap. is circular and concave, as in Tegulavis nov. gen. In contrast to the latter species, the coracoideum of Nanortyx shows a prominent processus procoracoideus that projects dorsally, and a fac. art. hum. that weakly protrudes laterally. Sobniogallus albinojamrozi Tomek et al., 2014 is a Galliforme, Family incertae sedis, described from the early Oligocene of Poland. Tegulavis nov. gen. resembles this genus in the laterally protruding fac. art. hum., which is separated from the shaft by a deep groove on the lateral surface. However, in Sobniogallus, the processus acrocoracoideus is obliquely directed, strongly projecting omally, and not hooked in sternal direction (Tomek et al., 2014: fig. 3-2
Comparison with the Lithornithidae. The coracoideum of Tegulavis
nov. gen. shows some similarities with that of the palaeognathous
Lithornithidae, which are recorded in the late Paleocene
and early Eocene of North America and in the early Eocene of Europe (Mayr, 2017a). Shared features between Tegulavis nov. gen. and Lithornithidae include: deep subcircular cotyla scap.; fac. art. hum. well developed and strongly projecting laterally (Houde, 1988). Tegulavis nov. gen. differs from the Lithornithidae in the absence of a foramen nervi supracoracoidei. In addition, in the Lithornithidae, the processus lateralis is very elongate, obliquely extended compared to the long axis of the shaft, and straightened at the tip in omal direction. The processus lateralis is incompletely preserved in Tegulavis nov. gen. but it was probably not elongate,
based on the orientation of the fac. art. sternalis.
Comparison with the Sandcoleidae. The coracoideum of Tegulavis
nov. gen. shows some similarities with that of Eoglaucidium
pallas
Fischer, 1987, which is very abundant in the middle Eocene
levels of the Geiseltal, in Germany (Mayr, 2020). In both Eoglaucidium and Tegulavis nov. gen., the cotyla scap. is circular and the processus procoracoideus is absent. In Eoglaucidium however, unlike in Tegulavis nov. gen., the shaft of the coracoideum is very thin and elongate, the fac. art. hum. is less prominent laterally and the foramen nervi supracoracoidei is present.

Fred


Fig. 1. Tegulavis corbalani nov. gen., nov. sp. from La Borie (early Eocene; Southern France), right coracoideum MHNT.PAL.2021.12.13 (holotype) in medial (A), dorsal (B), lateral (C), ventral (D), omal (E), and sternal (F) views. Abbreviations: cs, cotyla scapularis; fac, facies articularis clavicularis; fah, facies articularis humeralis; fas, facies
articularis sternalis; ila, impressio lig. acrocoracohumeralis; ims, impressio m. sternocoracoidei. Scale bar: 1 cm.
1721048667186.png
 
Order Gastornithiformes Stejneger, 1885
Family Gastornithidae Fürbringer, 1888
Genus Gastornis Hébert, 1855
Gastornis laurenti Mourer-Chauviré and Bourdon, 2020.

Referred material: see Appendix A. The reconstructed skeleton
shows the bones that have been discovered in La Borie.

Remarks:

Comparison with Gastornis parisiensis Hébert, 1855. The
humerus BR 12137 from Mont Berru (Fig. 5(H)) has been described
and illustrated by Martin (1992: fig. 3A, B). It is slightly larger
(147 mm in length) than those of G. laurenti (139.6 and
139.0 mm in length). The proximal part of the humerus is proximally shorter and dorsoventrally wider than in G. laurenti. On the cranial face, the crista deltopectoralis is obliquely oriented in the ventral direction. It protrudes above the surface of the shaft and does not end in a tubercle. On the caudal face, the fossa pneumotricipitalis is deeper than in G. laurenti, and the caput humeri forms a marked protuberance above this fossa. Small foramina are located below the caput humeri. The distal part is ventrally longer than in G. laurenti. The articular part is badly preserved but it seems that there was only one condyle, the triangular condylus dorsalis, as in G. laurenti.
A right femur from Cernay has been described by Lemoine
(1878). The extremities of this femur are very wide compared to
the shaft. The caput femoris strongly projects craniolaterally and
the fac. art. antitrochanterica is directed obliquely and cranially.
The structure including the crista tibiofibularis+tr. fibularis+lateral
crest of the tr. fibularis strongly projects laterally and distally,
which differs from G. laurenti (Fig. 6(A, B)). In addition, the condylus
lateralis is very thick on the cranial side (narrow in G. laurenti).
On the caudal side, the condylus medialis is badly preserved but it
seems strongly developed in proximodistal direction. A distal part
of right femur is known from Mesvin, Belgium (Dollo, 1883). This
femur also shows a very wide distal extremity compared to the
shaft and the crista tibiofibularis+tr. fibularis+incompletely preserved lateral crest of tr. fibularis strongly projects laterally and
distally. The condylus medialis is mediolaterally wide and its proximal outline is rounded. A proximal part of femur and a fragment of shaft are known from Croydon, England (Newton, 1890; Harrison and Walker, 1977). This fragment includes the incompletely preserved caput femoris and crista trochanteris, and the fac. art. antitrochanterica. The preserved part of the shaft is narrow compared to the proximal end. The caput femoris is more prominent medially and the collum femoris is more elongate than in G. laurenti. In the Croydon specimen the crista trochanteris is oriented toward the median axis of the bone, while in G. laurenti the crista follows its craniolateral border. Worthy et al. (2017) describe the condylus lateralis in G. parisiensis: ‘‘trochlea fibularis short and merges with side of condylus lateralis proximal to its distal end”.
This is true for the distal femur from Mesvin (Dollo, 1883), but
not for the femur from Cernay-lès-Reims (Lemoine, 1878: pl. I).
The holotype tibiotarsus of G. parisiensis, from Meudon, was figured by Owen (1856: pl. III, fig. 1a, 1b) and Milne-Edwards (1867-
68: pl. 28, figs. 1-4). These illustrations are slightly different, especially with regard to the distal view. In G. parisiensis the condylus medialis seems less prominent cranially and the pons supratendineus is narrower than in G. laurenti, but this is due to incomplete preservation. In the tibiotarsus from Croydon, on the caudal surface, both condyles are proximodistally elongate and caudally prominent. In the holotype tibiotarsus, the proximal part is not preserved. A proximal part of tibiotarsus n LR BR A4, fromthe Thanetian of Mont Berru, has been reported by Buffetaut (1997). In this specimen, the fac. art. medialis is obliquely oriented inmediodistal direction and the fac. art. lateralis is obliquely oriented in laterodistal direction,whereas in G. laurenti the fac. art.medialis is oriented proximally and the fac. art. lateralis is oriented caudally. In G. parisiensis, the sulcus between the articular surfaces (area interarticularis in Baumel and Witmer, 1993) is much wider that in G. laurenti and there is a large tubercle at the caudolateral angle of the fac. art. medialis, approximately in front of the fac. art. lateralis. This large tubercle is absent in G. laurenti,which shows a small tubercle in the craniolateral angle of the fac. art. medialis. Milne-Edwards (1867-68: p. 173- 174, pl. XXIX, figs. 4-5) described a fragment of fibula from Passy. This fragment corresponds to the middle part of the fibula, and the caput fibulae is not preserved. It consists of a flattened, rather thick blade, which is slightly curved craniocaudally. There is no crest on the lateral side, and no elongate fossa on the medial side, which strongly differs from G. laurenti (Fig. 6(F, G)). Two tarsometatarsi of G. parisiensis are known in the material from Mont Berru: a left one, unnumbered, from the Escuillié collection, a cast of which is preserved in the MNHN Paris collection (n L 3092), and a cast of right tarsometatarsus housed in the MNHN Paris (n L 3093). The left one has been described and figured by Angst (2014: fig. 27). These two specimens differ from that of La Borie (Fig. 7(A, B)) in the shape of the shaft: the medial and lateral sides are parallel, therefore the shaft does not show any narrowing (Martin, 1992: fig. 5A-F; Buffetaut and Angst: 2014, fig. 3B). The canalis interosseus distalis is open on the dorsal side in L 3092, but closed in L 3093. The tr. met. IV is elongate and extends beyond the mid-length of the tr. met. III. The tr. met. II does not show any groove. The incisura intertrochlearis medialis is narrower than in G. laurenti.
A phalanx 2 digit III of G. parisiensis from Mont Berru is very
similar to G. laurenti in size and proportion (Mourer-Chauviré
and Bourdon, 2016: tabl. 6; Table 1).
Comparison with Gastornis russelli Martin, 1992. This species is
known from a left tarsometatarsus and a tentatively referred
fragment of maxilla, both from Mont Berru. The holotype
tarsometatarsus (MNHN Paris R 3560) is very similar to G.
parisiensis, and only differs from the latter species in the smaller
size and slenderer shaft. Therefore, it differs from G. laurenti in
the same characters (Martin, 1992: fig. 6A-D, 7A). It shows a groove
instead of a closed canalis interosseus distalis. As noted previously,
measurements provided by Martin (1992) for this tarsometatarsus
are inaccurate (Mourer-Chauviré and Bourdon, 2016).
Comparison with Gastornis sarasini (Schaub, 1929). This species
comes from the locality of Monthelon (Schaub, 1929: figs. 1-4) and
is known from a distal fragment of tarsometatarsus bearing tr. met.
II and III, and a pedal phalanx. The measurements of the tarsometatarsus are close to those of G. laurenti. The canalis interosseus distalis is open on the dorsal side. The tr. met. III has an
expanded distal end. This feature is not visible in G. laurenti due to
the mediolateral crushing of this trochlea. G. laurenti differs from G.
sarasini in the closed canalis interosseus distalis, the tr. met. II oriented further medially and bearing a longitudinal groove. The fossa met. I is visible in G. sarasini, while it is not visible in G. laurenti due to crushing.
Comparison with Gastornis giganteus (Cope, 1876). The atlas of
G. laurenti (Fig. 4(A, B)) differs from that of G. giganteus in the elliptical shape of the foramen vertebrale (more rounded in G. giganteus), and in the laterally directed zygapophyses caudales
(dorsally directed in G. giganteus). In G. giganteus, Andors (1988:
p. 156) reports the presence ‘‘on the caudal side of the neural arch,
at the very base of each dorsal process, of subtriangular
zygapophyses” (see Matthew and Granger, 1917: pl. XXII, fig. 4c).
These subtriangular zygapophyses are absent in G. laurenti. The
axis of G. laurenti (Fig. 4(C, D)) differs from that of G. giganteus in
the following features: zygapophyses caudales more laterally elongate, processus costales less prominent, and, on the ventral surface of the arcus axis, area ligamenti elastici forming a depressed surface, while in G. giganteus it is slightly raised.
The cervical vertebra (Fig. 4(E-H)) resembles the three anterior
cervical vertebrae of G. giganteus figured by Matthew and Granger
(1917: pl. XXIII, figs. 2-4), but it is proportionally more elongate. In
G. giganteus the cranial zygapophyses and cranial articular facies
are located in cranial position, beyond the fac. art. cranialis. In contrast,
The cervical vertebra (Fig. 4(E-H)) resembles the three anterior
cervical vertebrae of G. giganteus figured by Matthew and Granger
(1917: pl. XXIII, figs. 2-4), but it is proportionally more elongate. In
G. giganteus the cranial zygapophyses and cranial articular facies
are located in cranial position, beyond the fac. art. cranialis. In contrast, these structures are located in more caudal position in G. laurenti. In G. giganteus, the processus costales ‘‘are quite vestigial,
represented only by a small knob below the anterior zygapophysis
with a little backwardly directed spine” (Matthew and Granger,
1917: p. 313). In contrast, the coastal processes are well developed
in G. laurenti.
The caudal vertebra of G. laurenti (Fig. 4(I, J)) also resembles the
caudal vertebra of G. giganteus figured by Matthew and Granger
(1917: pl. XXVII, fig. 4a, b). In this vertebra, the processus spinosus
is strongly widened at the tip. The fac. art. cranialis is circular in
shape, whereas it is bean-shaped in G. laurenti.
The humeri of G. laurenti (Fig. 5(A-F)) are smaller than the
humerus of the specimen AMNH 6169 from North America (total
length, 165.6 mm; Andors, 1988; Fig. 5(G)). In G. giganteus the
proximal part of the humerus is less ventrally curved, whereas
the distal part is more so than in G. laurenti. The tuberculum ventrale is proximally prominent. The caput humeri is obliquely elongate and forms a small protuberance above the wide and shallow fossa pneumotricipitalis. There is a small notch between the tuberculum ventrale and the caput humeri, which corresponds to the incisura capitis. On the cranial face, the oblique crista deltopectoralis slopes ventrally and ends in a tubercle, which is located approximatively in the middle of the shaft. According to Andors (1988: p. 200), this character is not present in all specimens of G. giganteus. The crista deltopectoralis forms a well-developed ridge in some individuals, especially in AMNH 6169, but only a low
rugosity in some others (Andors, 1988). The distal part of the
humerus is more dorsoventrally elongate than in G. laurenti. ‘‘The
internal and external condyles are small and poorly defined, and
there is only a faintest trace of a fossa olecrani” (Andors, 1988:
pp. 200-201), but both condyles are still present, whereas the
condylus ventralis is absent in G. laurenti. The incompleteness of the ulna from La Borie (Fig. 5(I, J)) does not allow meaningful comparisons. In G. giganteus, the shaft of the radius is straight and its proximal half is roughly circular in cross-section, ‘‘whereas its distal part is ancono-palmarly depressed, trigonal in section and broader owing to the outgrowth of a long and prominent external crest” (Andors, 1988: p. 203). In G. laurenti (Fig. 5(K, L)) the distal part of the shaft is dorsoventrally compressed and does not show any external crest. In G. giganteus, the extremities of the femur are much widened compared to the shaft. The collum femoris is elongate and the caput femoris strongly projects medially, but not proximally, unlike in G. laurenti (Fig. 6(A, B)) and G. parisiensis. In the lateroproximal angle, the trochanter is very high and robust. In some specimens (Troxell, 1931), it is extended by a short ridge on the cranial surface of the shaft. The crista tibiofibularis+tr. fibularis +lateral crest of tr. fibularis extends further distally than the condylus medialis, but the whole structure is much less laterally oriented than in G. parisiensis and G. geiselensis. ‘‘The fac. art.
antitrochanterica slopes posterodistally and its posterior [caudal]
angle forms a thickened labrum which overhangs an excavation
of the shaft” (Andors, 1988: p. 216). In G. laurenti, the fac. art.
antitrochanterica also protrudes caudally along the median axis
of the bone, but this labrum is much more prominent and lies
above a deeper depression in G. giganteus. In the latter species,
the condylus medialis is larger than in G. laurenti. The fossa poplitea is located proximal to the condylus medialis, while in G. laurenti it extends further distally. In cranial and caudal views, a
deep notch occurs in the distal outline of the sulcus intercondylaris
(Matthew and Granger, 1917: pl. XXXI; Troxell, 1931: fig. 5),
whereas in G. laurenti this notch is much shallower, especially in
cranial view. In the tibiotarsi of G. giganteus ‘‘the fossae retrocristales [. . .] are separated from one another by an oblique ridge [. . .] which prior to distortion would probably have been anteroposterior in orientation”(Andors, 1988: p. 222). In contrast, there is no separation between the fossae retrocristales in G. laurenti (Fig. 6(E)). In G giganteus the fac. art. medialis is oriented proximally, as in G. laurenti. In G. giganteus, the fac. art. lateralis is oriented proximally but it is extended, on the caudal surface, by a bulbous lobe, and there is a rough surface for the insertion of the caput fibulae distal to this lobe. In contrast, in G. laurenti, the fac. art. lateralis is completely located on the caudal surface (Fig. 6(D, E, J, K)). In G. giganteus, the area interarticularis is wide and shallow (very narrow in G. laurenti). A prominent tubercle is present in the centre of the proximal articular surface (absent in G. laurenti, perhaps due to erosion). In G. giganteus, a prominent tubercle is located next to the pons supratendineus and proximal to the condylus lateralis. According to Andors (1988: p. 226), this tubercle corresponds to the attachment of the retinaculum extensorium tibiotarsi. In contrast, in G. laurenti there is no tubercle and the retinaculum is attached to an oval, flattened, and rough zone (Fig. 6(C)). In G. giganteus, the cranial border of the condylus medialis is sharp (in G. laurenti the cranial border is rounded). The epicondylus medialis is very prominent (weakly prominent in G. laurenti). On the caudal surface, the crista trochleae lateralis is lateromedially compressed and much thinner than its medial counterpart (in G. laurenti the crista trochleae lateralis is not compressed). In G. giganteus, the fibula shows a longitudinal crest on the lateral side and an elongate fossa on the medial side, as in G. laurenti (Fig. 6(F, G)). However, the fossa is shallower in the former species, probably because the bone has not been so strongly compressed. In G. giganteus, a shallow depression occurs on the lateral side of the caput fibulae, distal to the fac. art. femoralis; this depression does not exist in G. laurenti.
In the tarsometatarsus of G. giganteus ‘‘the proximal and distal
extremities are widely expanded with respect to the shaft, which
is narrowly constricted in its middle” (Andors, 1988: p. 235). In
G. laurenti the constriction is less pronounced and is located closer
to the distal extremity (Fig. 7(A, B)). In G. giganteus, both foramina
vascularia proximalia open into the surface of the fossa infracotylaris dorsalis, instead of opening separately into a narrow and elongate fossa. The canalis interosseus distalis is reduced to a partly closed groove in some specimens, and the foramen vasculare distale is sometimes absent. The tr. met. II is the smallest and the
shortest of the trochleae, while in G. laurenti both tr. met. II and IV
have almost the same size and length. In G. giganteus ‘‘the longitudinal axis of the middle trochlea is coincident with the medial border of the shaft” and ‘‘the median trochlea projects anteriorly well in front of the plane of the shaft” (Andors, 1988: pp. 241-242), while in G. laurenti the tr. met. III is coincident with the median axis of the bone and does not project much anteriorly. In G. giganteus, the axis of the tr. met. III is oriented craniolaterally to caudomedially in plantar view (Shufeldt, 1913: pl. LIII, figs. 9, 12),
whereas it is oriented craniocaudally in G. laurenti.
The phalanges 1 digit III attributed to G. giganteus show great
morphological differences. Some of them are hourglass-shaped,
with strong narrowing above the tr. art. and condyles projecting
on the medial and lateral surfaces. Some others are stout, with parallel medial and lateral sides, and weakly projecting condyles. Concerning G. giganteus, we base our comparison on the phalanx 1
digit III of the specimen AMNH 6169, the almost complete skeleton
described by Matthew and Granger (1917: pl. 32, fig. 3) under the
name Diatryma steini and synonymised with Gastornis giganteus
(Cope, 1876) by Mlíkovsky´ (2002). Other North American species
of Gastornis have been synonymised with Gastornis giganteus by
Angst (2014). However, we think that their phalanges 1 digit III,
such as those of Gastornis ‘‘Diatryma” regens (Marsh, 1894: fig.
1a-d), or Gastornis ‘‘Diatryma” ajax (Shufeldt, 1913: pl. 52, fig. 4;
pl. 53, fig. 8; pl. 54, fig. 13) do not belong to Gastornis giganteus
(Table 1). The phalanx 1 digit III of G. laurenti is very similar to that
of the specimen AMNH 6169, but has a smaller size. In contrast, the
phalanx of G. regens (Marsh, 1894) differs from that of G. laurenti in
the following characters: longer shaft, cotyla art. with two subequal
parts separated by a more pronounced ridge, distal part
heart-shaped in distal view (flattened in G. laurenti), distal condyles
slightly projecting medially and laterally. The phalanx of G. laurenti is also very different from that of G. ajax (Shufeldt, 1913): in this phalanx 1 digit III the dorsal and plantar surfaces are very wide, the shaft does not taper distally, the condyles of the tr. art. do not project externally or plantarly, and the intercondylar groove is very faint.
The phalanges 2 and 3 digit III from La Borie are smaller than
those of G. giganteus AMNH 6169 (Table 1). On average, their
dimensions only reach 84% of those of the North American form.
The proportions of the phalanx 2 are similar in the two species,
but the phalanx 3 is slightly shorter and wider in G. laurenti.
Comparison with Gastornis geiselensis (Fischer, 1978). A well
preserved femur is known in the Geiseltal (Fischer, 1978;
Hellmund, 2013). Both extremities are greatly widened compared
to the shaft. The caput femoris strongly projects medially. On the
cranial surface, the crista trochanteris protrudes medially. The
fac. art. antitrochanterica protrudes on the caudal surface. The
crista tibiofibularis+tr. fibularis+lateral crest of the tr. fibularis
strongly protrudes on the caudal and lateral sides. The condylus
medialis is much wider than in G. laurenti, and its proximal outline
is rounded (flat in G. laurenti). Lastly, the fossa poplitea is proximodistally longer than in G. laurenti (Fig. 6(A, B)).
Three tibiotarsi are also known in G. geiselensis (Fischer, 1962,
1978). Two right tibiotarsi show cnemial crests that strongly project
proximally, especially the crista cn. cranialis. The sulcus intercnemialis is very wide in one of the tibiotarsi (collection number Dia 22). The crista cn. lateralis curves evenly distally but in this specimen it extends laterally, probably following a break
(Fischer, 1978). It is not possible to see the details of the proximal
articular surface. The tibiotarsi of G. geiselensis differs from those of
G. laurenti in the following characteristics: cristae cnemiales much
more prominent proximally, presence of deep depressio epicondylaris lateralis (shallow in G. laurenti), presence of a distinct tubercle proximal to the condylus lateralis (no tubercle in G. laurenti). The condylus medialis does not extend as far distally as the condylus lateralis. This morphology corresponds to the shape of the proximal part of the tarsometatarsus, in which the cotylae are not at the same level. In G. laurenti, a gap is also present between the distal extremities of the condyles, but it is not as pronounced as in G. geiselensis
The tarsometatarsi of G. geiselensis are strongly broken and distorted
(Fischer, 1962: pl. V, figs. 9-10; 1978: pl. XI, fig. 7; Hellmund,
2013: fig. 7a, 8a). They are relatively short, with a very wide proximal
extremity, a wide distal extremity, and a narrow mid-shaft.
The cotyla lateralis is situated further distally than the cotyla medialis.
The rounded fossa infracotylaris dorsalis is not prolonged by a
sulcus extensorius. The tr. met. IV is very wide and almost as long
as the tr. met. III. The tr. met. II is much shorter than the tr. met. IV
and is laterally curved at its base. G. geiselensis strongly differs from
G. laurenti in these characteristics. In addition, in G. geiselensis the
canalis interosseus distalis is open on the dorsal side, whereas it is
closed in G. laurenti. A reconstruction of a Geiseltal tarsometatarsus
was proposed by Hellmund (2013: fig. 7c, 8c).
A phalanx 1 digit III of G. geiselensis is reported but not figured
(Fischer, 1978); its measurements seem to correspond to an
hourglass-shaped phalanx because the minimal width of the distal
shaft is much inferior to the proximal width (Table 1). In this character, the phalanx 1 digit III of G. geiselensis probably looks similar to that of G. laurenti (Fig. 7(C, D)).
Comparison with Gastornis sp. from Louvois. A fragment of
proximal part of humerus has been reported from the late Paleocene locality of Louvois (Mourer-Chauviré and Bourdon, 2016:
fig. 2f). This fragment corresponds to a much larger humerus than
that of G. laurenti, but this difference is not a distinctive character
since the Gastornis sp. from Louvois shows an important sexual size
dimorphism (Mourer-Chauviré and Bourdon, 2016). As in G.
parisiensis
, small foramina are located beneath the distal edge of
the caput humeri, whereas these foramina are absent in G. laurenti.
The phalanx 2 digit III of the large form from Louvois is shorter
than that of G. laurenti (Table 1), the proximal part is wider, the
shaft is more constricted in the middle and the condyles of the
tr. art. are very faint on the plantar surface (Mourer-Chauviré
and Bourdon, 2016: fig. 3m, n). In both phalanges 3 digit III of
the large form from Louvois, the tr. art. shows barely distinct condyles. The lateral fovea lig. coll. is deep, circular in shape, and
extends far proximally onto the lateral surface, whereas the medial
fovea lig. coll. is shallow (Mourer-Chauviré and Bourdon, 2016: fig.
3o-r). In contrast, in the La Borie specimen the articular condyles
are distinct on the plantar surface, and both foveae lig. coll. are
shallow.
Comparison with Gastornis (Hou, 1980). A distal extremity of
tibiotarsus has been described in the early Eocene of China, and
is now attributed to the genus Gastornis (Buffetaut, 2013). G.
xichuanensis
differs from G. laurenti in its very large size. In the former species, the depth of the condylus medialis is only slightly
greater than the distal width, which gives to the distal articular
surface an almost square shape. In G. xichuanensis, the condylus
medialis projects only slightly cranially, while it is more prominent
in G. laurenti and would be even more so if the bone had not been
crushed on its medial side. Lastly, in G. xichuanensis the incisura
intercondylaris is deep and V-shaped, whereas in G. laurenti it is
wide, shallower and with a flat bottom.
Estimation of body mass and life reconstruction of Gastornis laurenti (Fig. 8). The body mass of G. laurenti can be estimated based on the least shaft circumference of the femur MHNT.
PAL.2018.20.2, and tibiotarsus MHNT.PAL.2018.20.3, by using the
regression equations of Campbell and Marcus (1992) for the AL
group. The results are 178 kg based on the femur and 190 kg based on the tibiotarsus. Angst (2014: table 2) indicates a mean mass of 145 kg based on the femora (n = 2), and 149 kg based on the tibiotarsi (n = 6), for G. parisiensis. However, the sample used by this author probably includes some tibiotarsi of G. laurenti. G. giganteus is heavier, with a mean body mass estimate of 210 kg based on the femora (n = 3), and 180 kg based on the tibiotarsi (n = 3). Concerning G. geiselensis, the width of the femur at mid-height is 54 mm (Fischer, 1962). It seems that this width corresponds to the least shaft width, therefore the body mass can be estimated to 205 kg

Fred


Fig. 1. Reconstructed skeleton of Gastornis laurenti Mourer-Chauviré and Bourdon, 2020. The right femur and tibiotarsus are thin because they have been strongly compressed craniocaudally
1721123245738.png

Fig. 2
Gastornis laurenti Mourer-Chauviré and Bourdon, 2020 from La Borie (early Eocene; Southern France). A, B. Atlas MHNT.PAL.2018.20.8 in cranial (A) and caudal (B) views. C, D. Axis MHNT.PAL.2018.20.9 in dorsal (C) and ventral (D) views. E-H. Vertebra cervicalis MHNT.PAL.2018.20.10 in dorsal (E), ventral (F), cranial (G) and caudal (H) views. I, J. Vertebra caudalis MHNT.2018.20.12 in cranial (I) and caudal (J) views. K. Fragment of pygostylus MHNT.2018.20.13 in cranial view. Abbreviations: ale, area ligamenti elastici; faat, facies articularis atlantica; faax, facies articularis axialis; faca, facies articularis caudalis; facr, facies articularis cranialis; fc, fossa condyloidea; fv, foramen vertebrale; if, incisura fossae; lp, lamina pygostyli; ps, processus spinosus. Scale bars: 2 cm.
1721123408585.png

Fig. 3. A-F, I-L. Gastornis laurenti Mourer-Chauviré and Bourdon, 2020 from La Borie (early Eocene; Southern France). A-E: right humerus MHNT.PAL.2018.20.6 in caudal (A), dorsal (B), cranial (C), proximal (D) and distal (E) views; F: left humerus HNT.PAL.2018.20.7 in caudal view; I, J: right ulna NT.PAL.2018.17.3 in ventral (I) and dorsal (J) views; K, L: shaft and distal part of right radius MHNT.PAL.2018.17.4 in dorsal (K) and ventral (L) views. G. Gastornis giganteus (Cope, 1876), right humerus AMNH 6169 in
cranial view. H. Gastornis parisiensis Hébert, 1855, right humerus BR 12137 in cranial view. Abbreviations: cd, crista deltopectoralis; cod, condylus dorsalis; fp, fossa
pneumotricipitalis; tav, tuberculum aponeurosis ventralis; tv, tuberculum ventrale. Scale bar: 3 cm.
1721123582703.png


Fig. 85 Life reconstruction of Gastornis laurenti (author: Guy Le Roux). The bird is eating some fruits of Anacardiaceae, remains of which have been identified in the paleoflora of La Borie (Laurent et al., 2010).
1721149172931.png
 
Order Gruiformes (Bonaparte, 1854)
Cf. Family Aramidae Bonaparte, 1849
Genus Papulavis nov.
LSID of new genus: 0807A8A1-00BF-457F-A28FCAD8014F2A09.

Derivation of the name: from Papulus, hermit and martyr who
lived during the Vth or VIth century and gave his name to the locality of Saint-Papoul, and avis, bird.

Type and only species: Papulavis annae nov. gen., nov. sp.

Stratigraphic and geographic range: Ypresian (early Eocene),
southern France

Diagnosis: As for the species Papulavis annae, by monotypy.

Papulavis annae nov. gen., nov. sp.
Fig. 9(A-D, F, H)
LSID of new species: AA72688D-B952-48C9-8AB7-
2761C38A2098.

Derivation of the name: This species is dedicated to Anne Hauradou, who actively participated in the fieldworks in the fossiliferous locality of La Borie.

Holotype: MHNT.PAL.2021.12.14, almost complete left
tarsometatarsus.

Type locality: La Borie, Saint-Papoul, Department of Aude,
Southern France.

Type horizon: Middle Ypresian, early Eocene, close to reference-level MP 8–9. Unlike remains of Gastornis, which have been found in the lenticular deposits SP1, SP2 and SP5, this fossil comes from the level SPO, located at the top of the quarry and corresponding
to a sandy channel.

Differential diagnosis: Tarsometatarsus elongate, but stouter
than in other Gruoidea; cotyla medialis more proximal than cotyla
lateralis; eminentia intercotylaris prominent and rounded; hypotarsus showing the configuration of ridges, canals and furrows
typical of Aramidae and distinct from that of extant Psophiidae and
Gruidae; relative length of trochleae closer to that of Aramidae and
Gruidae; tr. met. IV more strongly projected plantarly than in
Psophiidae, and less so than in Gruidae; differs from recent Aramidae in the size and position of the foramen vasculare distale, this foramen being smaller and located further away from the incisura intertrochlearis lateralis than in Aramus.

Remarks:
Comparison with extant Gruoidea. The hypotarsus exhibits the
peculiar morphology of the Gruoidea and differs from that of the
Ralloidea. The Gruoidea include the families Gruidae, Aramidae
and Psophiidae, and the Ralloidea include the families Rallidae,
Sarothruridae and Heliornithidae (Mayr, 2016a, 2019b). The
Aramidae include a single genus and species, Aramus guarauna,
the Limpkin, which lives in the Neotropics, from Georgia and Florida to central Argentina (Del Hoyo et al., 1996). The hypotarsus of Papulavis nov. gen. resembles that of extant Aramidae, since it
shows the same structure of ridges, canals and furrows, including
a thin crista medialis that strongly projects plantarly (Mayr,
2016b: fig. 2c, h; Fig. 9(D-G)). In the Gruidae, the crista medialis
is dorsoplantarly shorter and mediolaterally wider than in Papulavis
nov. gen. In the Psophiidae, there is no closed canal for fdl, but
only a furrow for fdl, fpp2, and fp2. The fossa met. I is very shallow
in both Aramus and Papulavis nov. gen. The position and relative
length of the trochleae of Papulavis nov. gen. is closer to that of
Aramidae and Gruidae, and differs from that of Psophiidae, in
which the tr.met. II is less strongly projected plantarly (Mayr,
2016b: fig. 1g, k; Fig. 9(H, I)). This trochlea is more strongly projected plantarly in the Gruidae than in the Aramidae and Papulavis nov. gen. In recent Aramidae the foramen vasculare distale is large and located very close to the incisura intertrochlearis lateralis, while in Papulavis nov. gen. this foramen is smaller and located further away from the incisura.
Comparison with extinct Aramidae. The only Paleogene forms
referred to the Aramidae include Badistornis aramus Wetmore,
1940, from the early Oligocene of South Dakota, and Loncornis erectus Ameghino, 1899, from the late Oligocene of Argentina. Badistornis aramus is known from an almost complete left tarsometatarsus (Wetmore, 1940; Cracraft, 1973: fig. 43). This is not certain whether this tarsometatarsus belongs to the Aramidae because the hypotarsus is not preserved. Papulavis nov. gen. differs from Badistornis in the less marked plantar orientation of the tr. met. II. The holotype of Loncornis erectus, originally described as a bird femur, has been identified as a fragment of mammalian humerus (Agnolín, 2008). Accordingly, the name Loncornis erectus is now considered as a nomen dubium. Another Paleogene taxon that was considered as an Aramidae is Aminornis excavatus Ameghino, 1899 from the late Oligocene of Argentina. Aminornis excavatus, described on the basis a fragmentary coracoideum, was referred to the Gruidae by Ameghino (1899). Brodkorb (1967) placed Aminornis in the Aramidae without explanation, and Cracraft (1973; see also Tonni, 1980) retained Aminornis in the Aramidae because he could not relocate the holotype. Agnolín (2004) relocated the holotype of Aminornis and reassigned it to the Anatidae. Concerning the Neogene, a putative Aramidae is Anisolornis excavatus Ameghino, 1891, from the early-middle Miocene of Argentina. Anisolornis, described on the basis a distal tarsometatarsus, was originally assigned to the Phorusrhacidae. Later, it was tentatively assigned to the Phasianidae by Ameghino (1895). Brodkorb (1964) placed the genus in the Cracidae (see also Tonni, 1980) with the comment that it ‘‘possibly belongs in the Tinamidae”. Finally, Anisolornis has been assigned to the Aramidae (Cracraft, 1973), or has been placed close to the Psophiidae (Olson, 1985). Papulavis nov. gen. differs from Anisolornis in the shorter and more plantarly displaced tr. met. II. Morevoer, in Papulavis nov. gen., the plantar opening of the foramen vasculare distale is located more proximally (Cracraft, 1973: fig. 45). Another extinct species, Aramus paludigrus Rasmussen, 1997, has been described from the middle Miocene of Colombia. It is only known from an almost complete tibiotarsus (Rasmussen, 1997).
Comparison with the Parvigruidae. The Parvigruidae are probably
the sister taxon of crown group Gruoidea (Mayr, 2013). They
comprise the genus Parvigrus, including the species Parvigrus pohli
Mayr, 2005 from the early Oligocene of France, and the genus
Rupelrallus, including the species Rupelrallus saxoniensis Fischer,
1997 from the early Oligocene of Germany. In addition, ?Parvigrus
cf. pohli and ?Rupelrallus belgicus Mayr, 2013 have been reported
from the early Oligocene of Belgium (Mayr, 2013). The hypotarsus
is preserved in only one specimen of ?Parvigrus cf. pohli. It has no
closed canal for fdl and the largest ridge is the crista intermedia,
here called central hypotarsal crest, and not crista medialis
(Mayr, 2013: fig. 1x, 3v). According to Mayr (2013: p. 81; 2016a:
p. 202), the hypotarsus of the early Oligocene Parvigruidae resembles that of the Psophiidae. Papulavis nov. gen. differs from the Parvigruidae because its hypotarsus includes an almost closed
canal for fdl and a crista medialis that protrudes further plantarly
than the crista intermedia. The tr. met. II of Papulavis nov. gen. is
not as strongly oriented plantarly as in the Parvigruidae (Mayr,
2013: fig. 1bb-gg), especially ?Rupelrallus belgicus (Mayr, 2013:
fig. 2-l).
Comparison with Bumbanipes aramoides Zelenkov, 2021. This
while in Papulavis nov. gen. this foramen is smaller and located further away from the incisura.
Comparison with extinct Aramidae. The only Paleogene forms
referred to the Aramidae include Badistornis aramus Wetmore,
1940, from the early Oligocene of South Dakota, and Loncornis erectus Ameghino, 1899, from the late Oligocene of Argentina. Badistornis aramus is known from an almost complete left tarsometatarsus (Wetmore, 1940; Cracraft, 1973: fig. 43). This is not certain whether this tarsometatarsus belongs to the Aramidae because the hypotarsus is not preserved. Papulavis nov. gen. differs from Badistornis in the less marked plantar orientation of the tr. met. II. The holotype of Loncornis erectus, originally described as a bird femur, has been identified as a fragment of mammalian humerus (Agnolín, 2008). Accordingly, the name Loncornis erectus is now considered as a nomen dubium. Another Paleogene taxon that was considered as an Aramidae is Aminornis excavatus Ameghino, 1899 from the late Oligocene of Argentina. Aminornis excavatus, described on the basis a fragmentary coracoideum, was referred to the Gruidae by Ameghino (1899). Brodkorb (1967) placed Aminornis in the Aramidae without explanation, and Cracraft (1973; see also Tonni, 1980) retained Aminornis in the Aramidae because he could not relocate the holotype. Agnolín (2004) relocated the holotype of Aminornis and reassigned it to the Anatidae. Concerning the Neogene, a putative Aramidae is Anisolornis excavatus Ameghino, 1891, from the early-middle Miocene of Argentina. Anisolornis, described on the basis a distal tarsometatarsus, was originally assigned to the Phorusrhacidae. Later, it was tentatively assigned to the Phasianidae by Ameghino (1895). Brodkorb (1964) placed the genus in the Cracidae (see also Tonni, 1980) with the comment that it ‘‘possibly belongs in the Tinamidae”. Finally, Anisolornis has been assigned to the Aramidae (Cracraft, 1973), or has been placed close to the Psophiidae (Olson, 1985). Papulavis nov. gen. differs from Anisolornis in the shorter and more plantarly displaced tr. met. II. Morevoer, in Papulavis nov. gen., the plantar opening of the foramen vasculare distale is located more proximally (Cracraft, 1973: fig. 45). Another extinct species, Aramus paludigrus Rasmussen, 1997, has been described from the middle Miocene of Colombia. It is only known from an almost complete tibiotarsus (Rasmussen, 1997).
Comparison with the Parvigruidae. The Parvigruidae are probably
the sister taxon of crown group Gruoidea (Mayr, 2013). They
comprise the genus Parvigrus, including the species Parvigrus pohli
Mayr, 2005 from the early Oligocene of France, and the genus
Rupelrallus, including the species Rupelrallus saxoniensis Fischer,
1997 from the early Oligocene of Germany. In addition, ?Parvigrus
cf. pohli and ?Rupelrallus belgicus Mayr, 2013 have been reported
from the early Oligocene of Belgium (Mayr, 2013). The hypotarsus
is preserved in only one specimen of ?Parvigrus cf. pohli. It has no
closed canal for fdl and the largest ridge is the crista intermedia,
here called central hypotarsal crest, and not crista medialis
(Mayr, 2013: fig. 1x, 3v). According to Mayr (2013: p. 81; 2016a:
p. 202), the hypotarsus of the early Oligocene Parvigruidae resembles that of the Psophiidae. Papulavis nov. gen. differs from the Parvigruidae because its hypotarsus includes an almost closed
canal for fdl and a crista medialis that protrudes further plantarly
than the crista intermedia. The tr. met. II of Papulavis nov. gen. is
not as strongly oriented plantarly as in the Parvigruidae (Mayr,
2013: fig. 1bb-gg), especially ?Rupelrallus belgicus (Mayr, 2013:
fig. 2-l).
Comparison with Bumbanipes aramoides Zelenkov, 2021. This
form is represented by a distal part of tarsometatarsus from the
early Eocene of the Bumban Mb., Mongolia (Zelenkov, 2021a: fig.
3c-e). This genus is assigned to Gruiformes incertae familiae, but
the author describes similarities with the recent genus Aramus,
which are expressed in the specific name aramoides. Papulavis
nov. gen. resembles Bumbanipes in the width of the shaft, the relative length of the trochleae, and the position of the foramen vasculare distale. It differs from the Mongolian form in the following characteristics: tr. met. III triangular in plantar view (almost square in Bumbanipes); tr. met. II more strongly oriented plantarly; tr. met. IV with a well-marked articular groove (less marked in Bumbanipes).

Fred


Fig. 9. A-D, F, H. Papulavis annae nov. gen., nov. sp. from La Borie (early Eocene; Southern France), left tarsometatarsus MHNT.PAL.2021.12.14 (holotype) in dorsal (A), plantar (B), medial (C), proximal (D) views, plantar view of the hypotarsus (F) and distal view (H). E, G, I. Recent species Aramus guarauna USNM 554 339, left tarsometatarsus in proximal view (E), plantar view of the hypotarsus (G), and distal view (I). Abbreviations: cmd, crista medialis hypotarsi; imc, crista intermedia hypotarsi. Scale bars: 1 cm.
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cf. Messelornithidae or cf. Walbeckornis
Fig. 10.

Material:
Almost complete left tibiotarsus, MHNT.PAL.2021.12.15.

Measurements (in mm): Total length, 59.0; proximal width, as
preserved, 3.8; proximal depth from cranialmost tip of crista cn.
lateralis to caudal border, 7.7; length of crista fibularis, 10.3;
mid-shaft width, 2.5; mid-shaft depth, 2.2; distal width, 5.1; depth
of condylus medialis, 4.8; depth of condylus lateralis, 4.5.
Almost complete left tibiotarsus, MHNT.PAL.2021.12.15

Remarks:
Comparison with the Messelornithidae. The Messelornithidae are medium-sized rail-like birds that are abundantly represented in the early Eocene of Messel (Hesse, 1988a, 1988b, 1990). The Messel species is Messelornis cristata Hesse, 1988. Two other species are known, Messelornis nearctica Hesse, 1992 from the middle Eocene of the Green River Fm., USA (Hesse, 1992; Weidig, 2010), and Messelornis russelli Mourer-Chauviré, 1995 from the late Paleocene of Mont Berru, France. Other messelornithids include Pellornis mikkelseni Bertelli et al., 2011 from the early Eocene of the Fur Fm., Denmark, and Itardiornis hessae Mourer-Chauviré, 1995 from the late Eocene and early Oligocene of the Phosphorites du Quercy, France. Other early Eocene Messelornithidae are known in the Nanjemoy Fm., USA, and in Ampe Quarry, near Egem, Belgium (Mayr, 2016c; Mayr and Smith, 2019a). The genus Walbeckornis, from the middle Paleocene of Walbeck, Germany, is probably not a messelornithid, but its phylogenetic affinities are uncertain (Mayr, 2017a). Other elements related to Messelornithidae or Walbeckornis are known in the middle Paleocene of Maret, Belgium, in the late Paleocene of Rivecourt-Petit Pâtis, France (Mayr and Smith, 2019b), and in the early Eocene of Mongolia (Zelenkov, 2021a). The tibiotarsus from La Borie exhibits the morphological characteristics of the Messelornithidae described by Hesse (1988a, 1988b, 1990).
However, it differs from Messelornis cristata in the wide sulcus
extensorius, which occupies most of the cranial surface of the distal
part of the bone, whereas the sulcus is situated on the medial
side in M. cristata. The specimen from La Borie also differs from
M. cristata in the larger distal opening of the canalis extensorius.
It is not possible to distinguish the features of the cranial surface
of the tibiotarsus in M. nearctica, however one can see that the
condylus medialis is distally flattened and cranially elongate
(Hesse, 1992: fig. 9). The tibiotarsus is unknown in M. russelli
(Mourer-Chauviré, 1995). In Pellornis mikkelseni ‘‘a short crista cnemialis lateralis projects underneath. A short but well projected
crista cnemialis lateralis is also present in other Messel rails”
(Bertelli et al., 2011: p. 559). We assume that the word ‘‘short”
must be understood as short in the proximodistal direction.
Hesse (1990: p. 94) also shows that the cristae cnemiales are proximodistally short in M. cristata. On a new specimen of P. mikkelseni, the distal outline of the condylus lateralis is rounded and slightly protruding on the caudal surface, and the condylus medialis is narrow and cranially elongate (Musser et al., 2019: fig. 3). The tibiotarsus from La Borie differs from Itardiornis (and Messelornis; see above) in the wider sulcus extensorius and larger distal opening Fig. 10. Cf. Messelornithidae or cf. Walbeckornis from La Borie (early Eocene; Southern France), left tibiotarsus MHNT.PAL.2021.12.15 in cranial (A), caudal (B), lateral (C), proximal (D), and distal (E) views. Abbreviations: ccl, crista cn. lateralis;
cf, crista fibularis; cl, condylus lateralis; cm, condylus medialis; se, sulcus extensorius. Scale bar: 5 mm. of the canalis extensorius. However, the first character shows some variability (Mourer-Chauviré, 1995: pl. 11, figs. 25, 28). Messelornithidae or closely related forms are present in the localities of Rivecourt-Petit Pâtis and Ampe Quarry near Egem, but the material does not include tibiotarsi (Mayr and Smith, 2019a, 2019b).
Comparison with Walbeckornis and Wanshuina. The tibiotarsus
from La Borie slightly resembles that of Walbeckornis creber
Mayr, 2007 from the upper middle Paleocene of Germany (Mayr,
2007). In the latter species, the crista cn. lateralis projects laterally
and ends in a sharp point. The sulcus extensorius is narrow in one
of the figured specimens (Fig. 4(H)), but wide in the other (Fig. 4
(G)). The distal edge of the pons supratendineus is thick. The tibiotarsus from La Borie differs from that of W. creber in the crista cn. lateralis that extends further laterally. The distal part of the Walbeck tibiotarsus is widened medially (vs. not widened in the specimen from La Borie), and the distal opening of the canalis
extensorius is small (vs. wide in the specimen from La Borie). In
the specimen WAL 390.2007 (Fig. 4(H)), a small ridge occurs
between the lateral margin of the pons supratendineus and the lateral tuberositas retinaculi extensori. This ridge does not exist in the specimen from La Borie. A form related to Walbeckornis is also present in the middle Paleocene of Maret, Belgium, but it is only
known from a distal tarsometatarsus (Mayr and Smith, 2019b).
The genus Wanshuina has been described from the Paleocene of
China (Hou, 1994). In Wanshuina, in contrast to the tibiotarsus
from La Borie , the distal end of the tibiotarsus is medially widened,
the sulcus extensorius is very deep, the incisura intercondylaris is
very wide, the condylus medialis is slightly obliquely oriented relative to the long axis of the shaft, and the epicondylus medialis is very prominent. Bumbaniralla walbeckornithoides Zelenkov, 2021
from the early Eocene of Mongolia, is related to both Walbeckornis
and Messelornithidae, but it is only known from an omal part of
coracoideum (Zelenkov, 2021a: fig. 3f-h).
Comparison with the Songziidae. The Songziidae are closely
related to the Messelornithidae. They have been described from
the early Eocene of China with the genus Songzia (Hou, 1990;
Wang et al., 2012). In France, an avian fossil designated as cf.
Songziidae gen. and sp. indet. has been reported from the middle
or upper Paleocene of Menat (Mayr et al., 2018). In Germany, a
Songziid-like bird has been described from the early Eocene of
Messel, with the genus Vanolimicola (Mayr, 2017b). Two undescribed fossils from the early Eocene of the Green River Fm., USA, show some similarity with Vanolimicola (Mayr, 2017b). Lastly, a? Songziidae gen. and sp. indet. has been reported from the early
Eocene of Driftwood Canyon, British Columbia, Canada (Mayr
et al., 2019). Morphological details of the tibiotarsi are not preserved in the Songziidae or closely related forms. The cristae cnemiales are generally not visible. These are ‘‘only moderately
prominent” in the Menat form (Mayr et al., 2018: p. 578), which
differs from the specimen from La Borie. However, in Vanolimicola
‘‘the condylus medialis is fairly large and its proximodistal length
exceeds the minimum mediolateral width of the tibiotarsus shaft”
(Mayr, 2017b: p. 145), which is also the case in the tibiotarsus from
La Borie. The main characteristic of these forms is their small size,
and the fact that their leg (especially the tibiotarsus) is proportionally very elongated relative to their size.
Size comparison. The total length (59 mm) of the tibiotarsus
from La Borie lies within the size range of Messelornis cristata
(mean 61.4 mm, n = 138, extremes 54.0–69.5 mm; Hesse, 1988a)
and also within the size range of the largest specimens of M. nearctica (54.9–67.2 mm; Weidig, 2010). The tibiotarsus from La Borie is smaller than in Pellornis mikkelseni (69.1 mm; Musser et al., 2019). The total length is unknown in M. russelli and I. hessae, but the other dimensions are larger than in M. cristata (Mourer-Chauviré, 1995). The main difference is that the tibiotarsus from La Borie is proportionally thinner and longer that in the species of Messelornithidae.Its robustness index (100 mid-shaft width / total
length) equals 4.24, while it equals 6.35 in M. nearctica (Hesse,
1992). Mid-shaft width is not provided for the other species, but
if this dimension is measured on the figures, the robustness index
is always above 6.00. The tibiotarsus from La Borie is larger than
that of Walbeckornis creber (estimated length 48 mm; Mayr,
2007) but, according to the dimensions measured on Fig. 4(D),
the robustness index equals 4.89 in Walbeckornis, which is close
to that of the specimen from La Borie. In the Songziidae and related forms the total length of the tibiotarsus varies from 27/28.5 mm in the Menat species to 40/40.3 mm in Songzia acutunguis (Wang et al., 2012). The Songziidae and related forms are therefore clearly smaller than the species from La Borie.

Fred


Fig. 10. Cf. Messelornithidae or cf. Walbeckornis from La Borie (early Eocene; Southern France), left tibiotarsus MHNT.PAL.2021.12.15 in cranial (A), caudal (B), lateral (C), proximal (D), and distal (E) views. Abbreviations: ccl, crista cn. lateralis;
cf, crista fibularis; cl, condylus lateralis; cm, condylus medialis; se, sulcus extensorius. Scale bar: 5 mm.
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Aves incertae sedis

Material:
almost complete right clavicula, MHNT.PAL.2018.17.1
(Fig. 11(B)); omal part of left clavicula, MHNT.PAL.2018.17.2
(Fig. 11(A)).

Measurements (in mm; first measurement for the right clavicula,
second one for the left clavicula): Length, as preserved, 133.4–
91.8; length from extremitas omalis claviculae to fac. art. acrocoracoidea: 23.2–26.4; craniocaudal depth of processus acromialis: 8.3–7.9; mediolateral width of scapus claviculae: 15.1–13.0; craniocaudal depth of scapus claviculae:

Remarks: It is not possible to assign these claviculae to any of
the taxa already identified in La Borie locality. Little is known about
the claviculae of the genus Gastornis. Concerning G. giganteus, ‘‘all
that remains of the clavicle [in AMNH 6169] is a broken stump
which overhangs the internal distal angle at and below the level
of the glenoid” (Andors, 1988: p. 194). This fragment is anteromedially convex and posterolaterally concave. A fragment of clavicula, fused to the scapulocoracoid, is known in G. parisiensis (Martin, 1992: fig. 3). The omal part of this clavicula forms a wide surface, with a medial crest that continues the medial border of the scapula. This omal part of clavicula is completely fused to the scapula and omal part of the coracoideum, and its lateral face is concave. It delimits a groove that passes dorsally along the scapula and coracoideum. Farther distally, the clavicula forms a flattened blade that narrows gradually. The sternal end is missing, but it seems that this clavicula did not extend much farther sternally. The claviculae from La Borie cannot be attributed to the genus Gastornis, firstly because they are very different from what is known in G. giganteus and G. parisiensis, and secondly because their small size does not match the size of Gastornis laurenti, even for a juvenile individual of this species.
The La Borie avifauna also includes the genus Galligeranoides
Bourdon et al., 2016. This taxon was initially placed in the order
Gruiformes, family Geranoididae, but new elements made it possible to show that Galligeranoides is very close to the genus Palaeotis, described from the localities of Geiseltal and Messel (Mayr, 2019a). Therefore, Galligeranoides is now placed in the family Palaeotididae, and the genera Galligeranoides and Palaeotis form a clade of palaeognathous birds. Galligeranoides is only known from partial tibiotarsi and one tarsometatarsus, whereas Palaeotis is known from several subcomplete skeletons. In one of these skeletons (Peters, 1988), ‘‘rudimentary scapi claviculorum” can be seen (Mayr, 2015: p. 509). One can estimate the size of the clavicula based on the size of the coracoideum. In Palaeotis weigelti Lambrecht, 1928, the length of the coracoideum from the rocessus
procoracoideus to the sternal extremity equals 33 mm in the specimen HLMD Me 7530, and 43 mm in the specimen GM 4362
(Houde and Haubold, 1987). In the specimen HLMD Me 771, this
length can be estimated to 36 mm (Mayr, 2015: fig. 3a). The best
preserved clavicula measures about 140 mm. These indeterminate
claviculae are too large to be attributed to the genus Galligeranoides, which approximately matches Palaeotis in size. In addition, the claviculae from La Borie, which were probably fused to form a furcula, correspond to a flying bird. However, Palaeotis was a flightless bird, which suggests that the closely related taxon Galligeranoides was also probably flightless.
Although the La Borie avifauna is relatively poor and only
includes five taxa so far, it provides interesting elements of comparison with contemporaneous avifaunas. The most abundant
taxon in La Borie is the gigantic flightless bird Gastornis. This taxon
is represented by a new species, Gastornis laurenti, which has been
recently described based on the mandible, maxilla and quadrate
(Mourer-Chauviré and Bourdon, 2020). Postcranial elements also
show morphological differences with those of earlier (G. parisiensis
and G. russelli) and more recent (G. sarasini and G. geiselensis) European species, and with those of the North American species G.
giganteus
. In the genus Gastornis, a modification of the shape of
the tarsometatarsus can be observed through time. In the oldest
forms, G. parisiensis and G. russelli, the medial and lateral sides of
the shaft are parallel. Later on, the shaft narrows in the middle,
as in G. giganteus. At last, the tarsometatarsus becomes shorter
and strongly constricted in the middle, as in G. geiselensis. In G. laurenti, the actual length of the shaft is difficult to evaluate. However, the narrowing occurs closer to the distal part of the shaft, unlike in G. giganteus, in which the narrowing occurs at mid-length of the shaft. The fossiliferous localities that have yielded remains of Gastornis are relatively numerous in the Paleocene and in the early and middle Eocene of Northern Europe (Buffetaut and Angst, 2014;
Buffetaut and Ploëg, 2020), but some of these localities have not
yielded a rich avifauna. However, the avifaunas from the early
Eocene (Ypresian) of the London Clay (England), Egem (Belgium),
and Messel (Germany), as well as the middle Eocene (Lutetian) of
the Geiseltal (Germany), are very diversified. The La Borie avifauna
resembles those of Messel and Geiseltal in the presence of Gastornis, a Palaeotididae, and a small gruiform related to either Walbeckornis or Messelornithidae. It differs from those of Messel and Geiseltal in the absence of small arboreal forms, which are extremely abundant in these localities (Mayr, 2009, 2017a, 2020). It also differs from these coeval avifaunas in the presence of the putative galliform Tegulavis nov. gen., which does not resemble any of the other previously described galliforms. At last, it differs from those of Messel and Geiseltal in the presence of the genus Papulavis nov. gen., which is tentatively assigned to the family Aramidae. Extinct members of this family have not been previously reported in Europe. If the presence of an aramid-like species is confirmed by the discovery of new remains in La Borie, it would provide further evidence that numerous extant neotropical taxa were formerly widespread in the Northern Hemisphere. These taxa comprise for instance the Anhimidae, Cariamiformes, Opisthocomiformes, Steatornithidae, Nyctibiidae, Trochilidae, Momotidae, Todidae, Galbulae and Tyrannida (Blondel and Mourer-Chauviré, 1998; Mayr, 2011; Duhamel et al., 2020; Riamon et al., 2020). This possibility has already been mentioned by Mayr (2017a: p. 158), who wrote: ‘‘Because this record (in the Northern Hemisphere) includes putative gruoidean stem group representatives, Psophiidae and Aramidae possibly belong to the fair number of extant taxa with a relictual distribution in the Neotropic region”.
Outside Europe, the avifauna from La Borie can be compared
with that of the early Eocene of the Bumban Mb. of the Tsagaan
Khushuu locality in Mongolia. This avifauna includes abundant
remains of Presbyornithidae (stem group anseriforms), and a
Phoenicopterimorphae, which indicate an aquatic or semi-aquatic
habitat (Kurochkin and Dyke, 2011). In the Gruiformes, Bumbanipes
aramoides
Zelenkov, 2021 shows similarities with the recent genus
Aramus, and Bumbaniralla walbeckornithoides Zelenkov, 2021 is
related to Messelornithidae and to Walbeckornis. Among the terrestrial birds of the Bumban Mb. are two genera of stem group galliforms, and a very small strigiform (Kurochkin and Dyke, 2011;
Hood et al., 2019; Zelenkov, 2021a, 2021b). The avifauna from La
Borie resembles that of the Bumban Mb. in the presence of a stem
group galliform and two gruiforms including an aramid-like bird
and a messelornithid-like or Walbeckornis-like bird. However, the
avifauna from the Bumban Mb. differs from that of La Borie in
the presence of numerous aquatic forms and in the absence of large birds such as Palaeotididae and Gastornithidae.
Floristic and faunistic elements identified in La Borie made it
possible to propose a paleoenvironmental reconstruction consisting
of a strongly waterlogged alluvial flood plain where the water
could episodically become brackish. The climate was tropical, with
a poorly marked dry season. The vegetation was locally composed
of broad-leaved trees, but this vegetation was sparse due to frequent
floodings (Laurent et al., 2010). The avifauna matches well
with this paleoenvironmental reconstruction, since arboreal forms
are totally absent in La Borie so far. The living species Aramus guarauna, the Limpkin, lives in freshwater marshes and swamps, as
well as in mangroves (Del Hoyo et al., 1996). It forages in shallow
water and eats almost exclusively apple snails (Del Hoyo et al.,
1996), which belong to the genus Pomacea (Ampullariidae). Some
characters that distinguish Aramus from other Gruiformes are
related to its specialized diet (Del Hoyo et al., 1996). Therefore,
one can speculate that the distribution and evolutionary history
of Aramus and these exclusively neotropical apple snails are linked
to one another, which seems to conflict with an Old World fossil
record of Aramidae. However, the Limpkin also feeds on other
aquatic snails and mussels. In terrestrial habitats, its diet includes
land snails and a variety of other small preys (Del Hoyo et al.,
1996). Moreover, although there is no evidence that Pomacea was
present in the Eocene of Europe (Martín and De Francesco, 2006),
the aramid-like bird from La Borie could have fed on freshwater
snails with an ecological niche similar to that of this taxon. The
presence of an aramid-like bird in La Borie is in good agreement
with other floristic and faunistic elements from this locality
(Laurent et al., 2010).

Fred


Fig. 11. Indeterminate bird from La Borie (early Eocene; Southern France). A. Right clavicula MHNT.PAL.2018.17.1 in caudal view. B. Left clavicula MHNT. PAL.2018.17.2 in caudal view. Abbreviation: faa, facies articularis acrocoracoidea. Scale bar: 1 cm.
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